On the distribution of COâ and CO in the mesosphere and lower thermosphere
We have used the Whole Atmosphere Community Climate Model (WACCM) to calculate the distribution of COâ and CO in the mesosphere and lower thermosphere (MLT), and we have compared the results with observations, mainly from the Atmospheric Chemistry Experiment Fourier Transform Spectrometer and Michelson Interferometer for Passive Atmospheric Sounding satellite-borne instruments. We find that WACCM can reproduce the observed distribution of COâ in the MLT and the rapid falloff of COâ above about 80âkm. Analysis of the principal terms in the calculated budget of COâ shows that its global-mean vertical profile is determined mainly by the competition between molecular diffusive separation and eddy mixing by gravity waves. The model underestimates somewhat the mixing ratio of COâ in the thermosphere compared to that in the observations, but we show that the discrepancy may be eliminated by a reasonable adjustment of the Prandtl number used to calculate the diffusivity due to gravity waves. Simulated CO is also consistent with observations, except that in the standard version of the model, its mixing ratio is uniformly lower than observed above about 100âkm. We conclude that WACCM likely underestimates the rate of production of CO in the lower thermosphere from photolysis of COâ at wavelengths <â121ânm, and we show that this stems from the use of a very large absorption cross section for Oâ in the wavelength range 105-121ânm. When a smaller cross section is used, photolysis of COâ increases by a factor of 2-3 at ~â95-115âkm and, as a result, CO mixing ratios become larger and agree much more closely with observations. We emphasize that the increase in COâ photolysis implies only minor changes in the vertical profile of COâ because photolytic loss is a minor term in the budget of COâ in the MLT.
document
https://n2t.org/ark:/85065/d72v2h27
eng
geoscientificInformation
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publication
2016-01-01T00:00:00Z
publication
2014-05-16T00:00:00Z
Copyright 2014 American Geophysical Union.
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